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<br />Tables <br /> <br />II <br /> <br />III <br /> <br />IV <br /> <br />V <br /> <br />VI <br /> <br />VII <br /> <br />VIII <br /> <br />IX <br /> <br />x <br /> <br />XI <br /> <br />XII <br /> <br />XIII <br /> <br />XIV <br /> <br />XV <br /> <br />XVI <br /> <br />LIST OF TABLES <br /> <br />Estimate of scale changes during seeded periods with respect to non-seeded <br />periods as computed by three statistical methods. Scale changes are shown <br />as a function of the 500 mb temperature. <br /> <br />Estimate of scale changes during seeded periods with resp ect to non- seeded <br />periods as computed by three statistical methods. Scale changes are shown <br />as a function of the 700 mb mixing ratio. <br /> <br />Estimate of scale changes during seeded periods with respect to non-seeded <br />periods as computed by thre e statistical methods. Scale changes are shown <br />as a function of a computed vertical gradient of potential condensate in the <br />700-500 mb layer. <br /> <br />Estimate of scale changes during seeded periods with respect to non-seeded <br />periods as computed by three statistical methods. Scale changes are shown <br />as a function of the 700 mb equivalent potential temperature. <br /> <br />Estimate of scale changes during seeded periods with respect to non-seeded <br />periods as computed by three statistical methods. Scale changes are shown <br />as a function of the convective stability in the 700-500 mb layer (9E500- 9E700)' <br /> <br />Estimate of scale changes during seeded periods with respect to non-seeded <br />periods as computed by three statistical methods. Scale changes are shown <br />as a function of a computed mean temperature advection in the 700-500 mb <br />layer. <br /> <br />Estimate of scale changes during seeded periods with respect to non-seeded <br />periods as computed by three statistical methods. Scale changes are shown <br />as a function of the 700 mb wind direction. <br /> <br />Estimate of scale changes during seeded periods with respect to non-seeded <br />periods as computed by three statistical methods. Scale changes are shown <br />as a function of the 500 mb wind direction. <br /> <br />Estimate of scale changes during seeded periods with respect to non-seeded <br />periods as computed by three statistical methods. Scale changes are shown <br />as a function of the 700 mb wind speed. <br /> <br />EEjtimate of scale changes during seeded periods with respect to non-seeded <br />periods as computed by three statistical methods. Scale changes are shown <br />as a function of 500 mb wind speed. <br /> <br />Monthly and seasonal precipitation amounts (inches) and number of days <br />during which it fell at hour stations in the Upper Colorado River Basin <br />above Kremmling. <br /> <br />Three-seasonhistorical rel~ord of daily precipitation amounts at Berthoud <br />Pass which equaled or exceeded. 40 inch. <br /> <br />Three-season totals 0f storm days grouped by duration periods, San Juan <br />area. <br /> <br />Hourly precipitation, December 27-29, 1964 (hundredths of an inch). <br /> <br />Matrix of partial correlation coefficients of 9 stations located in the northern <br />and central Colorado Rockies. Sample consists of 545 daily precipitation <br />amounts for the period April - November. <br /> <br />Matrix of partial correlation coefficients of 14 stations located in southern <br />Colorado and extreme northern New Mexico. Sample consists of 379 daily <br />precipitation amounts for the period April - November. <br /> <br />vi <br /> <br />Page Number <br /> <br />16 <br /> <br />17 <br /> <br />18 <br /> <br />19 <br /> <br />20 <br /> <br />21 <br /> <br />22 <br /> <br />23 <br /> <br />24 <br /> <br />25 <br /> <br />47 <br /> <br />48 <br /> <br />48 <br /> <br />49 <br /> <br />49 <br /> <br />50 <br />